thermal impacts of engineering activities and vegetation layer on permafrost in different alpine ecosystems of the qinghai–tibet plateau, china
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2016
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Abstract
Climate warming and engineering activities have various impacts
on the thermal regime of permafrost in alpine ecosystems of the
Qinghai–Tibet Plateau. Using recent observations of permafrost thermal
regimes along the Qinghai–Tibet highway and railway, the changes of such
regimes beneath embankments constructed in alpine meadows and steppes are
studied. The results show that alpine meadows on the Qinghai–Tibet Plateau
can have a controlling role among engineering construction effects on
permafrost beneath embankments. As before railway construction, the
artificial permafrost table (APT) beneath embankments is not only affected by
climate change and engineering activities but is also controlled by alpine
ecosystems. However, the change rate of APT is not dependent on ecosystem
type, which is predominantly affected by climate change and engineering
activities. Instead, the rate is mainly related to cooling effects of railway
ballast and heat absorption effects of asphalt pavement. No large difference
between alpine and steppe can be identified regarding the variation of soil
temperature beneath embankments, but this difference is readily identified in
the variation of mean annual soil temperature with depth. The vegetation
layer in alpine meadows has an insulation role among engineering activity
effects on permafrost beneath embankments, but this insulation gradually
disappears because the layer decays and compresses over time. On the whole,
this layer is advantageous for alleviating permafrost temperature rise in the
short term, but its effect gradually weakens in the long term.
| Reference Key |
wu2016thethermal
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|---|---|
| Authors | ;Q. Wu;Z. Zhang;S. Gao;W. Ma |
| Journal | journal of applied polymer science |
| Year | 2016 |
| DOI |
10.5194/tc-10-1695-2016
|
| URL | |
| Keywords |
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